Las minas de Guelaya y la Guerra del Rif

En el archivo del Quaid’Orsay de París he podido consultar la correspondencia que entre 1907 y 1909 mantuvieron el embajador francés en Madrid y su ministro de Asuntos Exteriores. Aunque existe bibliografía sobre los acontecimientos que condujeron a la campa��a de 1909, la documentación de las cajas 88-95 (Affaires duRif) de la Correspondance politique et militaire posee una doble virtud: detalla esos acontecimientos y contribuye a esclarecer varios temas polémicos, razón por la que preparo un trabajo basado en esa correspondencia. Esta nota de investigación adelanta algunas de sus conclusiones. La he dividido en dos partes. En la primera, relato los sucesos que originaron la guerra y en la segunda utilizo la documentación para tratar dos temas controvertidos: el problema de las minas como desencadenante de la contienda y el papel que Alfonso XIII jugó en ella. La limitación de espacio que exige una nota de investigación me ha obligado a “comprimir” la primera parte y por la misma razón no he incluido notas a pie de página citando los documentos de donde proviene la información.

Geodynamic events reconstructed in the Betic, Maghrebian, and Apennine chains (central-western Tethys)

A synthetic study has been made to identify main tectono-sedimentary and geodynamic events in central-western Tethys. For this, an interdisciplinary analysis has been performed on successions belonging to tectonic units derived from Betic-Maghrebian-southern Apennine “Flysch basin” domain. The stratigraphic records of the internal, external, and mixed successions deposited in lateral basins of different chains show very similar characters, especially regarding: (a) lithostratigraphy and ages; (b) kind and provenance of supplies (immature and supermature petrofacies from internal and external margins, respectively); (c) presence of “mixed successions” (composed of alternating internal and external petrofacies) attesting to clear palaeogeographic relationships between opposite depositional systems; and (d) timing of the deformation. In addition, specific lithofacies reveal correspondence with similar sedimentary events, such as: (1) very thick silicoclastic supply concentrated in restricted time ranges indicating the main deformational phases in the margin/basin systems; (2) levels rich in black-shales, glauconian, siliceous-producers, and volcaniclastic intercalations, widespread in the studied successions and linked to particular events at the Tethyan scale (anoxic periods, starvation-upwelling, acid-intermediate penecontemporaneous volcanic activity, respectively). Tectonic influence has also been recorded by means of unconformities and tectofacies (such as turbidites, slumps, or olisthostromes, etc.), being correlated with the main deformational phases. Similar stratigraphic and tectonic events have also been found in the Calvana unit of Val Marecchia nappe (Ligurides, northern Apennine). Correlations of stratigraphic and tectonic events support the proposal of an evolutionary geodynamic model involving the presence of a “Mesomediterranean microplate” in intermediate position during Africa-Europe convergence. The closure of central-western Tethys occasioned the Betic-Maghrebian-southern Apennine oceanic branch deformation and the birth of perimediterranean chains during middle-late Miocene.